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Nilin Pavate EES 3.5

EES 3.5

TermDefinition
Temperature A measure of how hot or cold something is.
Humidity The amount of water vapor (moisture) in the air.
Circulation The large-scale movement of air or water that distributes heat around Earth.
Global winds Major wind systems that blow in consistent directions over long distances.
Jet stream A fast-moving ribbon of air high in the atmosphere that influences weather patterns.
Atmosphere The layer of gases surrounding Earth.
Ocean A large body of salt water covering most of Earth’s surface.
Air mass A large body of air with similar temperature and humidity throughout.
Cold front The boundary where a cold air mass pushes under and replaces a warm air mass.
Warm front The boundary where a warm air mass slides over a cold air mass.
Precipitation Any form of water that falls from clouds (rain, snow, sleet, hail).
Temperature gradient The rate at which temperature changes over a certain distance.
Hurricane A powerful tropical storm with strong winds and heavy rain that forms over warm ocean water.
Thunderstorm A storm with thunder, lightning, heavy rain, and sometimes hail or strong winds.
Convection Heat transfer by the movement of liquids or gases (warm rises, cool sinks).
Conduction Heat transfer through direct contact.
Radiation Heat transfer through energy waves (like heat from the Sun).
Pacific Ocean The largest ocean on Earth, located between Asia/Australia and the Americas.
Trade winds (Easterlies) Steady winds that blow from east to west near the equator.
Westerlies Winds that blow from west to east in the middle latitudes.
Global impacts Effects that influence the entire planet.
El Niño A climate pattern where unusually warm ocean water appears in the central and eastern Pacific, affecting global weather.
La Niña A climate pattern where ocean waters in the central and eastern Pacific are cooler than normal.
Warm ocean current A stream of warm ocean water that moves heat from the equator toward the poles.
Gulf Stream A warm Atlantic Ocean current that carries heat from the Gulf of Mexico toward Europe.
Coastal regions Areas of land located near the ocean.
Oceanic conveyor belt The global system of deep and surface ocean currents that circulate water around the planet.
Coriolis effect The apparent bending of moving objects (like wind and currents) caused by Earth’s rotation.
Heat Energy transferred from a warmer object to a cooler one.
Wind belts Large bands of global winds (trade winds, westerlies, polar easterlies).
Equator The imaginary line around Earth at 0° latitude, halfway between the poles.
Poles The northernmost and southernmost points on Earth (North Pole and South Pole).
Ocean gyres Large circular systems of ocean currents.
Thermohaline circulation Deep ocean circulation driven by differences in temperature (thermo) and salinity (haline).
Surface temperatures Temperatures measured at Earth’s surface (land or ocean).
Deep currents Cold, dense ocean currents that flow far below the surface.
Regional climate Cold, dense ocean currents that flow far below the surface.
Regional climate The typical weather conditions of a specific area over a long period.
Climate zones Large areas of Earth classified by typical temperature and precipitation patterns
Maritime Tropical (mT) Warm and humid; forms over tropical oceans.
Maritime Polar (mP) Cool and moist; forms over cold oceans.
Continental Tropical (cT) Hot and dry; forms over land in low latitudes.
Continental Polar (cP) Cold and dry; forms over land in high latitudes.
Continental Arctic (cA) Extremely cold and dry; forms over Arctic regions.
Seasons Periods of the year (spring, summer, fall, winter) caused by Earth’s tilt and orbit around the Sun.
Sea breeze A daytime wind that blows from the ocean toward land.
Coastal fog Thick fog that forms near coastlines when moist air cools.
Hurricanes Large tropical cyclones with strong winds and heavy rain.
Local climate The typical weather conditions in a small, specific area.
Moisture content The amount of water vapor in the air.
Land-sea breezes Local wind systems caused by temperature differences between land and water (sea breeze by day, land breeze by night).
Hadley Cells Large circulation cells where warm air rises near the equator and sinks around 30° latitude.
Upwelling The rising of cold, nutrient-rich water from deep in the ocean to the surface.
Downwelling The sinking of surface water to deeper parts of the ocean.
Earth’s rotation The spinning of Earth on its axis, which causes day and night.
Atmosphere The layer of gases surrounding Earth that supports life and protects the planet.
Created by: user-1995925
 

 



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